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Clerical:
Themes of the Day:
Limestones & Dolostones
- Sea-Level Curves
- Overview of Carbonates
- Carbonates - (CO3)2- - 10-15% of all sed rocks
- Acid reaction - CaCO3+2HCl=Ca2++2Cl-+CO2+H2O
- often quite pure - only minor clays, silica as impurities - Why? Think: depositional environments
- Textures - more important for classification because of minimal chemical variability
- Grain Types (allochemical particles)
- Matrix
- Grain Size, Sorting, Rounding
- Insoluble Residues - chert nodules
- Classification
- Structures
- Depositional Environments
- CaCO3 Equilibria
- CaCO3+CO2+H2O=Ca2++2H++2CO32-
- Temperature effect - CO2 solubility is key
- Shaken, not stirred - soda/beer/champagne
- Salinity - lessens CO2 solubility
- Organic activity - photosynthesis (plants) vs. respiration (animals)
- Soil Zone
- Diagenesis
- Dolostones
- Dolostone Environments of Formation
- Geochemistry of Dolomite - CaMg(CO3)2
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